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Transition from MODIS AOD  VIIRS AOD

Transition from MODIS AOD  VIIRS AOD. Robert Levy (NASA-GSFC) Shana Mattoo , Leigh Munchak (SSAI @ NASA-GSFC) Falguni Patadia (GESTAR/Morgan State Univ. @ NASA-GSFC) Lorraine Remer (JCET-UMBC). VIIRS-2013 College Park, MD, November 2013. Aerosol retrieval from MODIS.

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Transition from MODIS AOD  VIIRS AOD

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  1. Transition from MODIS AOD  VIIRS AOD Robert Levy(NASA-GSFC) Shana Mattoo, Leigh Munchak(SSAI @ NASA-GSFC) FalguniPatadia (GESTAR/Morgan State Univ. @ NASA-GSFC) Lorraine Remer (JCET-UMBC) VIIRS-2013 College Park, MD, November 2013

  2. Aerosol retrieval from MODIS May 4, 2001; 13:25 UTC Level 2 “product” What MODIS observes Attributed to aerosol (AOD) May 4, 2001; 13:25 UTC Level 1 “reflectance” OCEAN GLINT LAND AOD 1.0 0.0 There are many different “algorithms” to retrieve aerosol from MODIS Dark Target (“DT” ocean and land; Levy, Mattoo, Munchak, Remer, Tanré, Kaufman) Deep Blue (“DB” desert and beyond; Hsu, Bettenhousen, Sayer,.. ) MAIAC (coupled with land surface everywhere; Lyapustin, Wang, Korkin,…) Ocean color/atmospheric correction (McClain, Ahmad, …) Etc (neural net, model assimilation, statistical, … ) Your own algorithm (many groups around the world)

  3. A MODIS view of global aerosol system (over dark targets)Collection 5 As envisioned by Y. Kaufman and D. Tanré And produced by the MODIS-aerosol team at NASA GSFC AOD Remer et al, 2008 We have two sophisticated sensors (aboard Terra and Aqua), with stable orbits, excellent calibration teams and validated aerosol retrievals. But we always want to do better.

  4. Diverse users of MODIS AOD: • Designed for use in climate research • Level 3 (gridded) for understanding global climate system: radiative forcing, global transport, aerosol/cloud interactions, geo-biology, etc. • Adapted for regional air quality monitoring • Level 2 (ungridded) for understanding regional air quality, regional transport, urban studies, etc • Adapted for assimilation and aerosol forecasting • Level 2 (ungridded) with error analysis to fill in model holes •  All have different data requirements for accuracy, usability, etc.

  5. Why has MODIS AOD has been so successful? • Yoram • MODIS was “new” (big jump from AVHRR) • Algorithm developers are also data users • Data are useful/accessible even if not perfect  user community “invested” into improvement process • Nearly 14 years since launch has created a huge community; tools and knowledge grew from zero (grassroots). • Lorraine and Shana  team continuity. • Reprocessing (traceable and consistent)

  6. MODIS Collection 6: Improvements Published in AMT • Levy, R. C., Mattoo, S., Munchak, L. A., Remer, L. A., Sayer, A. M., Patadia, F., and Hsu, N. C.: The Collection 6 MODIS aerosol products over land and ocean, Atmos. Meas. Tech., 6, 2989-3034, doi:10.5194/amt-6-2989-2013, 2013. http://www.atmos-meas-tech.net/6/2989/2013/

  7. Example of C6 changes: Aerosol over ocean

  8. Dark target over ocean Overall changes to products (Aqua, Jul 2008) • Overall decrease of AOD in mid-latitudes • Strong decrease in “roaring 40s” (even stronger in other months) • Overall increase in tropics • Coverage over inland lakes • Coverage toward poles

  9. Why the changes?

  10. C6-C5 ocean: Due to many incremental changes(Aqua, July 2008) New reflectance, geo-location inputs, Wisconsin cloud mask Re-define land and sea Updated radiative transfer • Also changed “Quality Assurance” Filtering • Changed aerosol definitions of land and sea • Etc Account for wind speed impact on surface Improved cloud mask

  11. Lessons learned from MODIS C6 development • There is always new “science” to implement • Iterating upon the “operational” environment allows for detailed testing • It is not just about “our” retrieval algorithm and product, it is also about “upstream” processing and products (e.g. calibration is very important) • Useful to have a friendly group of “beta-testers” • DETAILS ARE IMPORTANT!

  12. MODIS: Climate Data Records (CDRs)? “A time series of measurements of sufficient length, consistency, and continuity to determine climate variability and change.” Some requirements • Measurements sustained over decades • Measurement of measurement performance (e.g. calibration, stability) • Acquired from multiple sensors / datasets From: Climate Data Records from Environmental Satellites: Interim Report (2004) Have we sufficiently characterized the MODIS aerosol product? (whatever that means)

  13. MODIS instruments = “identical twins” Terra (10:30 Local Time, Descending) Aqua (13:30 Local Time, Ascending) • Like human twins: • Same parents (retrieval algorithm) for both instruments • But each MODIS has had a different life experience • (pre-launch, during-launch, during orbit) • They observe same world, but sample from different perspective • MCST works very hard to monitor both sensors • Two instruments, one world view?

  14. Global trends: If we had used Collection 5 • Over land, Terra decreases (-0.04/decade), Aqua constant • Terra / Aqua divergence is the same everywhere on the globe! • In NH, observations are 1.5 hours apart, while SH are 4.5 hours • So, probably not due to diurnal cycle of aerosol

  15. MCST improved “observed” reflectance for C6 • “Global” Aqua changes in visible bands by -0.001 or less • “Global” Terra changes in visible bands by +0.002 or more • Overall Aqua changes are relatively stable, but Terra’s changes vary over time. reflectance Difference reflectance

  16. Impact of New Terra calibration • Big changes to blue and red bands • Biggest impacts over land • Global increase by 0.02 (for this particular month). 10% of global mean! • Smaller impacts over ocean • Global increase by 0.004 (for this particular month)

  17. Impact of new calibration on trend • 8 months processed with same dark-target aerosol algorithms • Terra (T) Approach II now “in sync” with Aqua (A) time series • Aqua AOD reduced from 0.14 to 0.12over ocean • New calibration  Terra/Aqua divergence removed for C006! • (Terra-Aqua) offset remains 0.01 (ocean) and 0.015 (land)

  18. Beyond MODIS Suomi-NPP VIIRS Visible Infrared Imager Radiometer Suite Multiple VIIRS granules stitched. Image by Geoff Cureton, CIMSS Will VIIRS “continue” the MODIS aerosol data record?

  19. Orbit: 825 km (vs705 km), sun-synchronous, over same point every 16 days Equator crossing: 13:30 on Suomi-NPP, since 2012 (versus on Aqua since 2002) Swath: 3050 km (vs 2030 km) Spectral Range: 0.412-12.2m (22 bands versus 36 bands) Spatial Resolution: 375m (5 bands) 750m (17 bands): versus 250m/500m/1km Wavelength bands (nm) used for DT aerosol retrieval: 482 (466), 551 (553) 671 (645), 861 (855), 2257 (2113)  differences in Rayleigh optical depth, surface optics, gas absorption. Aerosol Retrieval: Created and maintained by scientists partnered with NOAA (NASA), with a strategy of maximizing environmentaldata record - EDR (climate data record – CDR) ALSO: Different cloud masks, different aggregation techniques, different pixel selections. VIIRS versus MODIS Aqua (13:30 Local Time, Ascending) Suomi-NPP (13:30 Local Time, Ascending);

  20. What if MODIS disappeared today? Will VIIRS “continue” MODIS? How would we know? Hsu et al., IF MODIS had died in 2012, we wouldn’t have much to work with. But VIIRS (and MODIS) teams have made major improvements

  21. Will VIIRS “continue” MODIS? How would we know? • Overall “validation” statistics compared with AERONET? • We know that Terra and Aqua have similar statistics, but we also see differences in global pictures, trends • According to VIIRS cal/val team, (after the early mission jitters and many changes), that V-EDR compared to AERONET is similar to MODIS-C5 compared to AERONET. • For next few slides, we work with data produced in March-May 2013 (after jitters and many changes). But we use MODIS C6 as a baseline

  22. Will VIIRS “continue” MODIS? How would we know? • Do they see the same world when overlapped? • Rare even with same equator crossing times

  23. Overlapping MODIS/VIIRS image over India (Mar 5, 2013, 0735 UTC) • Notes: • VIIRS “5 minute” granule stitched from four 86 sec granules • High quality QA data only Similar AOD structure Differences in: coverage magnitudes Why? 0.55 µm AOD -0.05 0.05 0.15 0.25 0.35 0.45 0.55 0.65 0.75

  24. IDP-VIIRS vs MODIS-C6 • Instrument/Algorithm • Swath/Orbit/Resolution/Wavelengths • Cloud mask / pixel selection strategy • Aggregation/Averaging (use of IP - retrieval) • Bowtie issues • Processing stream / granule size • Post-processing/Culture • File Format • Existence of Level 3 • Reprocessing • Near Real Time • Tools for data access • Research vs Operations • Climate vs Daily • NOAA versus NASA outreach

  25. Let’s homogenize as much as we can • Instrument/Algorithm • Swath/Orbit/Resolution/Wavelengths • Cloud mask / pixel selection strategy • Aggregation/Averaging (use of IP - retrieval) • Bowtie issues • Processing stream / granule size (with help from UW-PEATE) ONE RETRIEVAL ALGORITHM: CONSISTENT ACROSS PLATFORMS

  26. Run similar algorithm on VIIRS and MODIS (use “IFF” files) Much more similar AOD structure Still some differences in coverage/magnitude Why? 0.55 µm AOD -0.05 0.05 0.15 0.25 0.35 0.45 0.55 0.65 0.75

  27. Will VIIRS “continue” MODIS? How would we know? • Do overlapping granules look alike? • Even with same equator crossing, true space and time overlaps are rare (every 16 days, and only over India) • Now look “more” alike. We need to define how much “more” is good enough.

  28. Will VIIRS “continue” MODIS? How would we know? • Convergence of global mean (over land and ocean)? • Note that Terra and Aqua expected different by ±0.015. • What about seasonal cycle? • Convergence of global statistics? • Here, I am thinking about standard deviation, min, max, .. • How similar? • Convergence of global histogram? • Here, I am thinking about the “lognormal-like” shape of the retrieved distribution.

  29. Global Histogram convergence? March 2013 OCEAN Relative convergence of OCEAN (even V_EDR vs M_C6) 0.122 0.116 0.134 0.132 0.125 • M_C6 = MODIS C6 • ML_M = MODIS like on MODIS 1 km IFF • ML_V = MODIS like on VIIRS 750 km IFF • ML_V64 = ML_V filtered by VZA < 64° • V_EDR = VIIRS EDR LAND 0.244 0.249 0.258 0.259 0.239 Bigger differences over LAND (more similar for ML) Numbers in boxes are “global mean” Note few or no zeros/negatives for V-EDR

  30. Will VIIRS “continue” MODIS? How would we know? • Convergence of gridded (Level 3 –like) data? • For a day? A month? A season? • What % of grid boxes must be different by less than X in AOD?

  31. Convergence of Gridded Monthly? (Mar 2013) Different snow thresholds? Different SZA thresholds Handling of zero Still different, but much more similar over both land and ocean Step by step, we make ML_M and ML_V consistent.

  32. Will VIIRS “continue” MODIS? How would we know? • What about “sampling”? • Even if the mean, histograms and gridded data looked similar, what about the “retrievability?” • Fraction of retrieved pixels / total pixels

  33. Convergence of Monthly “retrievability” (Mar 2013) Are there places on the globe that cannot be retrieved by one satellite or another? Will they converge on cloud mask, pixel selection, availability of aerosol retrieval?

  34. Still not homogenized yet • Instrument/Algorithm • Swath/Orbit/Resolution/Wavelengths • Cloud mask / pixel selection strategy • Aggregation/Averaging (use of IP - retrieval) • Bowtie issues • Processing stream / granule size But maybe we can quantify the remaining differences We also need to run more months across MODIS / VIIRS record

  35. Summary (1) • There are many ways to retrieve aerosol properties from MODIS, and there is more than one set of algorithms/products • Dark-target algorithm/products are updated for C6 • Changes are “modest” but can lead to significant changes in retrieved global aerosol • The MODIS aerosol product has matured for >13 years • MODIS has become indispensable, and the community is not yet ready to adopt something new. MODIS RGB MODIS Aerosol (06:35 UT) MODIS RGB MODIS Aerosol (06:35 UT) The MODIS aerosol cloud mask is more conservative than the VIIRS VCM. The MODIS aerosol cloud mask is more conservative than the VIIRS VCM. VIIRS RGB MODIS Algorithm, VIIRS Input VIIRS Aerosol EDR VIIRS RGB MODIS Algorithm, VIIRS Input VIIRS Aerosol EDR

  36. Summary (2) • If MODIS died tomorrow • NPP-VIIRS is online • VIIRS is “similar”, yet different then MODIS • How different? • Can VIIRS continue the MODIS record? • Development of a common algorithm will help to quantify remaining differences between VIIRS and MODIS • We still need to define “how similar is good enough”? • Sorry, Lots of Questions, not many Answers! MODIS RGB MODIS Aerosol (06:35 UT) MODIS RGB MODIS Aerosol (06:35 UT) The MODIS aerosol cloud mask is more conservative than the VIIRS VCM. The MODIS aerosol cloud mask is more conservative than the VIIRS VCM. VIIRS RGB MODIS Algorithm, VIIRS Input VIIRS Aerosol EDR VIIRS RGB MODIS Algorithm, VIIRS Input VIIRS Aerosol EDR

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